Genesis of chlorine and sulphur in fumarolic emissions at Vulcano Island (Italy): assessment of pH and redox conditions in the hydrothermal system

Author:

Di Liberto V,Nuccio P.M,Paonita A

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference53 articles.

1. Special Field Workshop at Vulcano (Aeolian Islands) during summer 1988: Geochemical results;Badalamenti;Acta Vulcanol.,1991

2. Bale, C.W., Pelton, A.D., Thompson, W.T., 2001. Web F*A*C*T – Facility for the Analysis of Chemical Thermodynamics, http://www.crct.polymtl.ca/FACT/factwhat.htm, Ecole Polytechnique de Montréal, Montreal, QC.

3. The generation of HCl in the system CaCl2-H2O: Vapour-liquid relations from 380–500°C;Bischoff;Geochim. Cosmochim. Acta,1996

4. Isotopic variation of the hydrothermal system on Vulcano Island, Italy;Bolognesi;Geochim. Cosmochim. Acta,1993

5. Brimhall, G.H., Crerar, D.A., 1987. Ore fluids: Magmatic to supergene. In: Carmichael, I.S.E., Eugster, H.P. (Eds.), Thermodynamic Modeling of Geologic Materials: Minerals, Fluids and Melts. Rev. Mineral. 17, 235–322.

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